Schmiedl, Gerhard; Mackensen, Andreas (1997): Table A1. Age model of sediment core GeoB1214-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52769, In supplement to: Schmiedl, G; Mackensen, A (1997): Late Quaternary paleoproductivity and deep water circulation in the eastern South Altantic Ocean: Evidence from benthic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 130(1-4), 43-80, https://doi.org/10.1016/S0031-0182(96)00137-X
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Project(s):
Coverage:
Latitude: -24.690000 * Longitude: 7.240000
Date/Time Start: 1990-03-22T00:00:00 * Date/Time End: 1990-03-22T00:00:00
Minimum DEPTH, sediment/rock: 0.23 m * Maximum DEPTH, sediment/rock: 4.98 m
Event(s):
GeoB1214-1 * Latitude: -24.690000 * Longitude: 7.240000 * Date/Time: 1990-03-22T00:00:00 * Elevation: -3210.0 m * Recovery: 5.08 m * Location: Cape Basin * Campaign: M12/1 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: CC KS, weiß
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age model | Age model | ka | Schmiedl, Gerhard | Age model, SPECMAP chronology, Imbrie et al. (1984) | |
| 3 | Age, comment | Comm | Schmiedl, Gerhard | Marine Isotope Stage (MIS) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
64 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
|---|---|---|
| 0.23 | 12 | 2 |
| 0.48 | 28 | 3.1 |
| 0.73 | 53 | 3.3 |
| 0.78 | 65 | 4.2 |
| 0.93 | 80 | 5.1 |
| 1.03 | 87 | 5.2 |
| 1.18 | 99 | 5.3 |
| 1.33 | 107 | 5.4 |
| 1.53 | 122 | 5.5 |
| 1.63 | 128 | 6 |
| 1.73 | 135 | 6.2 |
| 1.78 | 146 | 6.3 |
| 1.83 | 151 | 6.4 |
| 1.88 | 171 | 6.5 |
| 1.98 | 183 | 6.6 |
| 2.08 | 186 | 7 |
| 2.18 | 194 | 7.1 |
| 2.23 | 205 | 7.2 |
| 2.33 | 216 | 7.3 |
| 2.53 | 228 | 7.4 |
| 2.58 | 238 | 7.5 |
| 2.63 | 249 | 8.2 |
| 2.78 | 269 | 8.4 |
| 2.88 | 287 | 8.5 |
| 2.98 | 299 | 8.6 |
| 3.18 | 310 | 9.1 |
| 3.43 | 331 | 9.3 |
| 3.63 | 341 | 10.2 |
| 3.93 | 362 | 11 |
| 4.48 | 405 | 11.3 |
| 4.83 | 423 | 12 |
| 4.98 | 434 | 12.2 |